Week 3 Lecture October 2001 Metabolism Continued Lecture Review Metabolism Basics Aerobic Metabolism of Organics This Week’s Lecture Anaerobic Respiration nitrate (NO3-), CO2, sulfate (SO42-), ferric iron (Fe3+), organics, and others Fermentation Syntrophic Association During Conversion of Mixed Acid Products to Methane Chemolithotrophy Photosynthesis Aerobic Respiration Overview carbon flows to carbon dioxide electrons flow to external acceptor energy produced by oxidative phosphorylation through PMF Respiration of Glucose glucose ADP ATP glycolysis pyruvate ½ O2 GDP GTP Citric Acid Cycle CO2 e- Electron Transport System Electrons flow in the form of reduced dinucleotides (NADH and FADH) H20 Question? What happens when the environment is anoxic or anaerobic? What is the difference between anaerobic and anoxic? What impact does this have on organic carbon biodegradation? What is the significance of these changes in environmental management and design? Anaerobic Respiration Some bacteria are capable of aerobic respiration and anaerobic respiration (aerobic is preferred due to more favorable energy production) Other bacteria that carry out anaerobic respiration are obligate anaerobes In either case, the electron acceptor chosen is based on maximizing free energy production for cell growth Anaerobic (Anoxic) Respiration of Organics Organic compounds are most often the original electron donor Most electron acceptors are inorganics Electron transport systems in anaerobic respiration is similar to that of aerobic metabolism Examples of Anoxic Respiration -0.50 increasing energy production NAD+/NADH2 So/HSCO2/CH4 SO4/S2Eo’ Fumarate/Succinate NO3- /NO2Fe3+/Fe2+ + 0.90 ½ O2/H20 terminal electron acceptors other than oxygen used less energy produced carbon flow the same as in aerobic respiration Nitrate Reduction (Denitrification) Conversion of nitrate (NO3-) as an electron acceptor to ammonia (NH4+) or nitrate (NO2-) Nitrite undergoes further reduction to produce nitric oxide (NO), nitrous oxide (N2O), and nitrogen gas (N2), all of which are lost to the atmosphere Denitrification results in a loss of nitrogen from ecosystems and is only carried out biologically by bacteria Nitrogen removal treatment processes incorporate denitrification Aerobic Respiration and Denitrification During aerobic respiration, three areas where H+ is pumped out to establish PMF Denitrification Only two areas in ETC that pump out H+ as compared to three for aerobic respiration Less energy generated Methanogenesis and Acetogenesis CO2 as an electron acceptor CO2 methanogenesis CH4 H2 acetogenesis acetate Sulfate Reduction sulfate (SO4)reduction to sulfide (S2-)requires eight electrons the first intermediate in this process is the production of sulfite (SO32-) and requires two electrons conversion of sulfite to sulfide requires an additional six electrons Sulfate Dissimilatory Reduction Why does sulfate inhibit methane formation? Hydrogen is needed for both processes Sulfate/sulfide (SO4/S2-) redox pair has a more positive reduction potential How would sulfate presence in an anaerobic digester affect methane formation? Iron Reduction Ferric iron (Fe3+) reduction to ferrous iron (Fe2+) Relatively large positive Eo’ indicates that Fe3+ is an attractive electron acceptor Ferrous iron is much more soluble and this process has been used in mining iron ore Because of the high concentrations of iron in some groundwaters, iron reduction is a common reaction in groundwater remediation Very little Fe3+ in surface waters at neutral pH Other Metals as Electron Acceptors Mn+4 to Mn+2 Cr+6 to Cr+3 Cr+3 much less toxic and soluble and is precipitated out AsO43- to AsO33 important in drinking water and groundwater systems mining wastes SeO42- to SeO42 major problem in agriculture lands in California If there are no external electron acceptors?? Suppose there are no electron acceptors like nitrate, various metals, etc. What happens to the electrons associated with the organic carbon that is oxidized? How do cells handle this condition? What is this called? Fermentation organic compounds serve as both e donor and acceptor no externally supplied e donor oxidized and reduced products formed carbohydrates are primary fermentable substrates ATP production occurs via substrate level phosphorylation Fermentation Fermentation reactions are important in: wastewater treatment processes phosphorus removal sludge digestion BOD removal wetland systems, especially in bottom sediments (PCB dechlorination) agricultural management plans for manure landfill leachate management Fermentation Carbon and Energy Flow Organic Compound e donor P substrate level phosphorylation ADP ATP intermediate intermediate ~P electron carrier Oxidized Organic intermediate e acceptor Reduced Organic fermentation product Pyruvic Acid Fermentation ADP ATP organics pyruvic acid NAD+ NADH NADH NAD+ acetaldehyde + CO2 NADH lactic acid NAD+ ethanol mixed acids Mixed Acid Fermentation Complex Organics propionic acid pyruvic acid acetic acid butyric acid formic acid CO2 H2 Mixed Acid Fermentation important in the breakdown of organic compounds in anaerobic environments primary products are organic acids, carbon dioxide, and hydrogen Conversion of Mixed Acid Fermentation Products to Methane acetic acid and carbon dioxide are converted to methane in anaerobic environments hydrogen is consumed in the process butyric and propionic acid are not converted directly to methane Methane Formation propionic acid pyruvic acid acetic acid CH4 butyric acid formic acid CO2 H2 Methane Formation propionic acid pyruvic acid butyric acid DGo’ + DGo’ + acetic acid CH4 formic acid CO2 H2 Mixed Acid Conversion to Acetic Acid Breakdown of acids such as butyric and propionic to acetic is required prior to methane formation This breakdown is energetically nonfavorable at standard conditions How do organisms alter the environment to achieve this reaction? Non-Standard Conditions DG = DGo’ + RT ln ([C][D]/[A][B]) Conversion of butyric and propionic acids results in acetic acid and H2 H2 is consumed by methanogens in the conversion of both acetic acid and CO2 to methane The reduction in H2 makes these reactions possible by lowering the product concentrations in the above equation Syntrophic Association Where a H2 producing organism can only grow in the presence of a H2 consuming organism The coupling of H2 formation and use is called interspecies hydrogen transfer If H2 builds up in a process it is indicative of an unbalanced consortium A H2 build-up will result in a build up of acids resulting in pH decreases and process failure Fermentation Summary Little free energy available for growth for example in glucose fermentation to ethanol, 2 moles of ATP produced/mole of glucose Most energy is tied up as products (alcohols, acids, methane, H2) These products produced as intermediate electron acceptors are reduced A key intermediate is pyruvate Can other substances besides organic carbon serve as electron donors? Chemolithotrophy the oxidation of inorganics for production of cellular energy terminal electron acceptor is typically oxygen most lithotrophs are also autotrophs accordingly, during lithotrophy there is a need to not only produce energy in the from of ATP but also reduced electron carriers to reduce CO2 to cell carbon Electron Flow in Lithotrophs CH2O CO2 NADP+ e- donor oxid e- donor e- e- e- Electron Transport Chain NADPH ADP ATP O2 energy gained from e- flow through ETC is used to drive reverse electron transport against an unfavorable reduction potential to form NADPH and then reduce CO2 H20 Electron Donors for Chemolithotrophy -0.50 2H+/H2 S0/HSSO42-/HS- 0.0 NH2OH/NH4+ Eo’ NO3- /NO2- the greater the reduction potential differences between the donor and oxygen, the greater the energy available for growth Fe3+/Fe2+ + 1.00 ½ O2/H20 primary electron acceptor for lithotrophy Hydrogen Oxidation chemolithotrophs use hydrogen as an energy source for growth those bacteria that use hydrogen as an electron donor and oxygen as a terminal acceptor are referred to as hydrogen bacteria (versus methanogens) Typically these bacteria are autotrophs that convert carbon dioxide to cell carbon via the Calvin cycle. The energy for this comes from oxidation of hydrogen using oxygen as an electron acceptor 6H2 + 2O2 + CO2 CH20 + H2 0 Sulfur Oxidation Oxidation of hydrogen sulfide (H2S), elemental sulfur (So) and thiosulfate (S2O32-) Final Product is sulfate (SO42-) Very important in acid mine drainage, biological corrosion Sulfur Oxidation Reactions H2S + 2O2 So + H20 + 1/2O2 S2O32- + H20 + 2O2 HS- + 1/2O2 + H+ SO42- + H+ SO42- + 2H+ 2SO42- + 2H+ So + H20 sulfur storage as granules Iron Oxidizing Bacteria At neutral pH and ambient conditions, ferrous iron (Fe2+) oxidizes quickly to ferric iron (Fe3+) Under acid conditions this reaction does not occur spontaneously Lithotrophs (Iron bacteria )biologically convert Fe2+ to Fe3+ under these conditions 4Fe2+ + O2 + 4 H+ 4 Fe3+ + 2 H20 Oxidation of iron results in little energy production because reduction potential of to Fe3+ /Fe2+ is so close to that of oxygen/water Nitrification Conversion of ammonium (NH4+) to nitrate (NO3-) Nitrite (NO2-) is an intermediate Nitrification is a very important process agriculturally as it leads to the oxidation of ammonia to nitrate and potential nitrogen loss through denitrificiation In wastewater treatment, nitrification is often needed to reduce the oxygen demand the effluent Nitrification Reactions Nitrosomonas NH4+ + 3/2O2 NO2- + H20 + 2H+ Nitrobacter NO2- + 1/2O2 NO3- Oxidation of ammonia results in production of acidic conditions Very little energy available to nitrifiers because reduction potential relatively close to that of oxygen Energy Production During Phototrophy the ability to photosynthesize is based on light sensitive pigments called chlorophylls all cells have chlorophyll A and typically some others photosynthesis converts light energy to chemical energy chemical energy produced is used for cell growth in phototrophs which typically are autotrophs (energy is required to reduce CO2 to cellular carbon) photosynthesis occurs in both anaerobic and aerobic environments Anoxygenic Photosynthesis energy production in anoxygenic photosynthesis occurs as a result of electron flow through an electron transport chain electron flow is cyclic membrane mediated process is similar to that in aerobic respiration and some electron transport components are common to both systems Electron Flow and Energy Production in Anoxygenic Photosynthesis P870 Center act. eElectron Transport Chain -0.60 Eo’ e- + 0.40 Antenna pigment complex P870 Center e- PMF ADP ATP Schematic of Anoxygenic Photosynthesis Photoautotrophs Phototrophs tend to be autotrophs As such, there is a need to reduce inorganic carbon (CO2) to organic carbon reducing power CO2 CH2O To reduce CO2 to organic carbon takes reducing power (NADPH) Autotrophs use reverse electron transport to produce NADPH Use of External Electron Acceptors in Anoxygenic Photosynthesis Electron Transport Chain P870 Center act. e- Antenna pigment complex P870 Center NADP+ e- e- ePMF NADPH ADP ATP e- H2S Oxygenic Photosynthesis involves two distinct but interconnected photoreaction centers electron flow is non-cyclic water is the primary electron donor as water is oxidized, oxygen is liberated in Eukaryotic organisms oxygenic photosynthesis occurs in chloroplast membranes in Prokaryotic organism, oxygenic photosynthesis occurs in cytoplasmic membrane Oxygenic Photosynthesis NonCyclic Electron Flow -1.0 NADP+ e- e- NADPH Eo’ e+ 0.8 H20 PMF 1/2O2 and 2H+ ATP ADP Phototrophy Summary Use of light energy to produce chemical energy in the form of ATP and reduced electron carriers ATP is used for normal cellular functions and to reverse normal electron flow where necessary to produce reduced electron carriers reduced electron carriers are used to reduce CO2 to organic carbon (Calvin Cycle) NADPH CO2 NADP+ CH2O